ClimateSearch

Nagoya, Aichi

Japan · 2.3M people · 23 m elevation · Northern Hemisphere

Every month in detail

Thirty-year averages for each calendar month.

Monthly climate normals. Values shown as an em dash are missing from the source data.
MonthJanFebMarAprMayJunJulAugSepOctNovDec
Average high48°F (9°C)50°F (10°C)58°F (14°C)68°F (20°C)77°F (25°C)82°F (28°C)88°F (31°C)92°F (33°C)84°F (29°C)74°F (23°C)63°F (17°C)53°F (12°C)
Average low33°F (1°C)34°F (1°C)40°F (4°C)49°F (10°C)58°F (15°C)67°F (19°C)74°F (24°C)76°F (25°C)69°F (21°C)58°F (15°C)47°F (8°C)38°F (3°C)
Dew point29°F (-2°C)29°F (-1°C)35°F (2°C)45°F (7°C)55°F (13°C)64°F (18°C)72°F (22°C)72°F (22°C)66°F (19°C)55°F (13°C)44°F (7°C)34°F (1°C)
Rainfall3.1 in (78 mm)3.3 in (84 mm)5.2 in (131 mm)6.7 in (171 mm)7.2 in (183 mm)9.1 in (231 mm)10 in (254 mm)6.3 in (160 mm)8.7 in (220 mm)7.3 in (186 mm)3.8 in (96 mm)3 in (76 mm)
Rainy days671011101111810976
Snowfall0.4 in (1.1 cm)1.3 in (3.2 cm)0 in (0.1 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0.2 in (0.5 cm)
Sunshine186 h169 h189 h178 h175 h127 h155 h206 h162 h169 h165 h180 h

Scroll the table sideways for all twelve months.

Projected change, 2031–2050

Model projection, not an observation

How this city’s climate may change, measured against the same models’ own 1995–2014 output. Nothing here affects the match score above.

Change in summer afternoon highs

+2.3°F (+1.3°C)

Models range from +1.8°F (+1.0°C) to +2.9°F (+1.6°C)

Days above 90°F (32°C) a year

14 → 40

About 2.8× as many

Warming by month
  • January: +2.3°F (+1.3°C)
  • February: +1.9°F (+1.1°C)
  • March: +1.8°F (+1.0°C)
  • April: +2.3°F (+1.3°C)
  • May: +2.0°F (+1.1°C)
  • June: +2.1°F (+1.2°C)
  • July: +2.5°F (+1.4°C)
  • August: +2.2°F (+1.2°C)
  • September: +2.6°F (+1.5°C)
  • October: +2.7°F (+1.5°C)
  • November: +2.5°F (+1.4°C)
  • December: +2.2°F (+1.2°C)
Scenario
SSP5-8.5 (high emissions)
Models
4 · CMIP6 HighResMIP, downscaled

This is a high-emissions pathway — the upper end of plausible futures, not a central estimate. Changes are measured by each model against its own past output and then applied to the observed record, which cancels each model’s bias but not the genuine uncertainty about how much warming occurs. Where the models disagree widely, the range above is the honest answer.